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Progress in Earth and Planetary Science
Fig. 5 | Progress in Earth and Planetary Science

Fig. 5

From: Interannual variation of the Warm Arctic–Cold Eurasia pattern modulated by Ural blocking and the North Atlantic Oscillation under changing sea ice conditions

Fig. 5

Winter horizontal temperature advection pattern related to reversed winter sea ice change over the BKS. Similar to Fig. 4, but for winter horizontal temperature advection (shading; °C/day) and wind (vector; m/s) at 850-hPa. Dots in a–c denote shading statistically significant at the 0.05 level by Student's t test. The grey shadings in denote the topography

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